power point presentation on social science -interior of earth
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INTERIOR OF
EARTH
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Interior of earthThere are many limitations in collecting
information about the mysteries of the Earth'sinterior directly.
The temperature and pressure inside the Earthincreases with depth. The variations in pressureis due to the weight exerted by the overlying
layers.
The temperature at the centre of the Earth isabout 5000O C. emember that even iron meltsat !5"#O C.
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Interior of earthThe di$erent sources from which we get
information on the Earth's interior.
%rom the materials reaching the Earth'ssurface through volcanic eruptions.
&ata collected from mines.
nalysis of the propagation of wavesgenerated during earth(ua)es etc.
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Interior of earthOn the basis of varying density ad otherphysical and chemical properties of roc)sthe earth can be divided in to mainlythree there are
!. Crust
*. +antle
". core
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Interior of earth
CRUSTMANTLE
OUTER CORE
INNER CORE
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CRUSTThe comparatively
thin outer shell ofthe Earth.
pproximately ,0)m thic).
Two parts-continental crustoceanic crust.
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CRUSTContinental crust and oceaniccrustAs silica and alumina are the
chief contents,the continental crust is also
known asSIAL.As silica and magnesium are the
chief contents,
the oceanic crust is also known
asSIMA.
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MANTLE
Located beneath the crust.
Extends upto 29 !"
#ro" the crust.
T$o parts% upper "antle&
lo$er "antle.
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MANTLE'pper "antle
Upper mantle
The upper mantle, made
up of silicon compounds,is in a solid state.
.
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MANTLE
Lower mantle
The lower mantle,located beneath the
upper mantle, is in a
semi-liuid state
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CORE
Central part ofthe Earth.
%rom */00 )m to"1! )m
Two parts- outer
core inner core.
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CORE
Outer core andinner core
The materials inthe outer coreare in a moltenstate.
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CORE
Due to the highpressureprevailing at thecentre, the innercore is in a solidstate.
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CORE
As it is mainly
made up of theminerals nickel(Ni) and iron(Fe), it is also
known as NF!.
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Thank you